Through the Dark Continent, Vol. 2 (of 2) : $b or, The sources of the Nile around the Great Lakes of Equatorial Africa and down the Livingstone River to the Atlantic OceanStanley, Henry M. (Henry Morton)
History
Through the Dark Continent, Vol. 2 (of 2) : $b or, The sources of the Nile around the Great Lakes of Equatorial Africa and down the Livingstone River to the Atlantic Ocean
Stanley, Henry M. (Henry Morton)
Africa, Central -- Description and travel; Stanley, Henry M. (Henry Morton), 1841-1904 -- Travel -- Africa, Central
This was of itself conclusive proof that there was _no_ current at this
date (July 16, 1876). Still I was curious to see the river flowing out.
The next day, therefore, accompanied by the chief and fifteen men of the
Expedition, we started overland along the banks of this rush- and mud-
choked depression for three or four miles. The trend of the several
streams we passed was from north-west to south-east—that is, towards the
lake. At Elwani village we came to the road from Monyi’s, which is used
by people proceeding to Unguvwa, Luwelezi, or Marungu on the other side
of the Lukuga. Two men from the village accompanied us to the Lukuga
ford. When we reached the foot of the hill, we first came to the dry bed
of the Kibamba. In the rainy season this stream drains the eastern
slopes of the Ki-yanja ridge with a south-east trend. The grass-stalks,
still lying down from the force of the water, lay with their tops
pointing lakeward.
From the dry mud-bed of the Kibamba to the cane-grass-choked bed of
Lukuga was but a step. During the wet season the Kibamba evidently
overflowed broadly, and made its way among the mateté of the Lukuga.
We tramped on along a path leading over prostrate reeds and cane, and
came at length to where the ground began to be moist. The reeds on
either side of it rose to the height of 10 or 12 feet, their tops
interlacing, and the stalks, therefore, forming the sides of a narrow
tunnel. The path sank here and there into ditch-like hollows filled with
cool water from 9 inches to 3 feet deep, with transverse dykes of mud
raised above it at intervals.
Finally, after proceeding some two hundred yards, we came to the centre
of this reed-covered depression—called by the natives “Mitwanzi”--and
here the chief, trampling a wider space among the reeds, pointed out in
triumph water indisputably flowing westward!
The water felt cold, but it was only 68° Fahr., or 7° cooler than the
Lukuga. I crossed over to the opposite or southern bank, on the
shoulders of two of my men. The bed was uneven; sometimes the men rose
until the water was barely over their ankles, then again they sank to
their hips. The trees I had noticed from the open creek stood on a point
projecting from the southern bank across the Mitwanzi, but they were now
dead, as the former dry tract had become quaggy. The name Lukuga clings
to the bed until a few miles west of Miketo’s, when it becomes known as
the Luindi, Ruindi, or Luimbi.
The Mitwanzi is still daily traversed without trouble by men, women, and
children.
We travelled another three miles along the Mitwanzi, until we came to
the southern end of the Ki-yanja ridge, for it is through the gap
between this and the Kihunga ridge, which terminates on the south bank,
that the Lukuga flows toward the west. Even here it was but a trivial
stream, oozing and trickling through a cane-grass grove.
Public-domain text, read in full here on John Shaqi.
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